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Indications of Transformation Products from Hydraulic Fracturing Additives in Shale-Gas Wastewater

机译:页岩气废水中水力压裂添加剂转化产物的指示

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摘要

Unconventional natural gas development (UNGD) generates large volumes of wastewater, the detailed composition of which must be known for adequate risk assessment and treatment. In particular, transformation products of geogenic compounds and disclosed additives have not been described. This study investigated six Fayetteville Shale wastewater samples for organic composition using a suite of one- and two-dimensional gas chromatographic techniques to capture a broad distribution of chemical structures. Following the application of strict compound-identification-confidence criteria, we classified compounds according to their putative origin. Samples displayed distinct chemical distributions composed of typical geogenic substances (hydrocarbons and hopane biomarkers), disclosed UNGD additives (e.g., hydrocarbons, phthalates such as diisobutyl phthalate, and radical initiators such as azobis(isobutyronitrile)), and undisclosed compounds (e.g., halogenated hydrocarbons, such as 2-bromohexane or 4-bromoheptane). Undisclosed chloromethyl alkanoates (chloromethyl propanoate, pentanoate, and octanoate) were identified as potential delayed acids (i.e., those that release acidic moieties only after hydrolytic cleavage, the rate of which could be potentially controlled), suggesting they were deliberately introduced to react in the subsurface. In contrast, the identification of halogenated methanes and acetones suggested that those compounds were formed as unintended byproducts. Our study highlights the possibility that UNGD operations generate transformation products and underscores the value of disclosing additives injected into the subsurface.
机译:非常规天然气开发(UNGD)会产生大量废水,必须对废水的详细成分进行充分的风险评估和处理。特别地,没有描述地质化合物的转化产物和公开的添加剂。这项研究使用一套一维和二维气相色谱技术对六个费耶特维尔页岩废水样品进行了有机成分分析,以捕获广泛的化学结构分布。遵循严格的化合物识别-置信度标准,我们根据化合物的推定来源对其进行了分类。样品显示出不同的化学分布,这些化学分布由典型的地质成因物质(碳氢化合物和mark烷生物标志物),公开的UNGD添加剂(例如烃,邻苯二甲酸盐(例如邻苯二甲酸二异丁酯)和自由基引发剂(例如偶氮二(异丁腈)))和未公开的化合物(例如卤代烃)组成,例如2-溴己烷或4-溴庚烷)。未公开的链烷酸氯甲基酯(丙酸氯甲酯,戊酸酯和辛酸酯)被确定为潜在的延迟酸(即那些仅在水解裂解后才释放酸性部分的酸,其速率可能受到控制),表明它们是故意引入的以在酸中反应。地下。相反,对卤代甲烷和丙酮的鉴定表明,这些化合物是作为意外的副产物形成的。我们的研究突出了UNGD作业产生转化产物的可能性,并强调了披露注入地下的添加剂的价值。

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  • 来源
    《Environmental Science & Technology》 |2016年第15期|8036-8048|共13页
  • 作者单位

    Helmholtz Zentrum Muenchen, Institute of Groundwater Ecology, Ingolstaedter Landstrasse 1 85764, Neuherberg, Germany;

    School of Engineering and Applied Science, Yale University, 9 Hillhouse Avenue, New Haven, Connecticut 06511, United States;

    Department of Civil & Environmental Engineering, Duke University, Hudson Hall, Box 90287, Durham, North Carolina 27705, United States;

    Fye Laboratory, Woods Hole Oceanographic Institution, Mail Stop No. 4, Woods Hole, Massachusetts 02543, United States;

    School of Engineering and Applied Science, Yale University, 9 Hillhouse Avenue, New Haven, Connecticut 06511, United States;

    Department of Civil & Environmental Engineering, Duke University, Hudson Hall, Box 90287, Durham, North Carolina 27705, United States;

    Department of Chemistry, University of Washington, Bagley Hall, Seattle, Washington 98195 United States;

    Nicholas School of the Environment, Duke University, Gross Chemistry, Durham, North Carolina 27705, United States;

    Department of Civil & Environmental Engineering, Duke University, Hudson Hall, Box 90287, Durham, North Carolina 27705, United States,Nicholas School of the Environment, Duke University, Gross Chemistry, Durham, North Carolina 27705, United States;

    Fye Laboratory, Woods Hole Oceanographic Institution, Mail Stop No. 4, Woods Hole, Massachusetts 02543, United States;

    Helmholtz Zentrum Muenchen, Institute of Groundwater Ecology, Ingolstaedter Landstrasse 1 85764, Neuherberg, Germany;

    School of Engineering and Applied Science, Yale University, 9 Hillhouse Avenue, New Haven, Connecticut 06511, United States;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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  • 正文语种 eng
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  • 入库时间 2022-08-17 13:59:13

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